000 AXNT20 KNHC 011750 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 105 PM EST SUN FEB 01 2009 TROPICAL WEATHER DISCUSSION FOR NORTH AMERICA...CENTRAL AMERICA...GULF OF MEXICO...CARIBBEAN SEA...NORTHERN SECTIONS OF SOUTH AMERICA...AND ATLANTIC OCEAN TO THE AFRICAN COAST FROM THE EQUATOR TO 32N. THE FOLLOWING INFORMATION IS BASED ON SATELLITE IMAGERY...METEOROLOGICAL ANALYSIS...WEATHER OBSERVATIONS...AND RADAR. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1715 UTC. ...THE ITCZ... THE ITCZ IS CENTERED ALONG 7N10W TO THE EQUATOR AT 26W AND ALONG THE EQUATOR TO 40W AND INTO NE BRAZIL NEAR 2S45W. SCATTERED MODERATE CONVECTION IS FROM THE EQUATOR TO 3N BETWEEN 27W-37W. SCATTERED MODERATE/ISOLATED STRONG CONVECTION IS FROM 1N-3N BETWEEN 38W-43W. ...DISCUSSION... GULF OF MEXICO... SOUTHERLY SURFACE RETURN FLOW IS ACROSS THE GULF OF MEXICO W OF 85W ON THE WRN PERIPHERY OF DUAL 1027 MB SURFACE HIGH PRESSURE CENTERS...ONE OVER THE CENTRAL FLORIDA PENINSULA NEAR OCALA AND THE OTHER IN THE W ATLC NEAR 32N73W. THE SURFACE RIDGE AXIS EXTENDS ACROSS THE SRN GULF TO INLAND OVER MEXICO NEAR TUXPAN. MULTI-LAYERED CLOUDS COVER THE ENTIRE GULF WITH A RELATIVELY COOLER AIR MASS IN PLACE. ALOFT...ZONAL WESTERLY FLOW DOMINATES WITH MODERATE SUBSIDENCE OBSERVED ACROSS THE SE GULF AND BAY OF CAMPECHE. CARIBBEAN SEA... A DEEP LAYERED TROUGH IS OVER THE W ATLC AND SUPPORTS A COLD FRONT EXTENDING FROM THE W ATLC WATERS ACROSS HISPANIOLA AND INTO THE CARIBBEAN AS A STATIONARY FRONT ACROSS SW HAITI TO OVER THE SRN COAST OF JAMAICA AND THEN INLAND OVER NRN NICARAGUA. SCATTERED SHOWERS ARE ALONG AND BEHIND THE FRONT WITHIN 90 NM ACROSS NRN HISPANIOLA...JAMAICA AND CENTRAL AMERICA N OF 14N WITH 15-20 KT N-NE WINDS OBSERVED BASED ON AN EARLIER QUIKSCAT PASS ACROSS THE NW CARIBBEAN THIS MORNING. ACROSS THE CENTRAL CARIBBEAN...LOW-LEVEL CONVERGENCE OF THE TRADES ARE GENERATING SCATTERED SHOWERS S OF 14N BETWEEN 68W-74W. UPPER DIFFLUENCE ASSOCIATED WITH A BROAD RIDGE OVER NRN SOUTH AMERICA IS ENHANCING THIS SHOWER ACTIVITY. ELSEWHERE IN THE UPPER LEVELS... STRONG SUBSIDENCE COVERS THE CARIBBEAN W OF A LINE FROM GUADELOUPE TO NE COLOMBIA. ATLANTIC OCEAN... A DEEP LAYERED TROUGH IS OVER THE W ATLC AND SUPPORTS A COLD FRONT THAT ENTERS THE DISCUSSION AREA NEAR 32N52W EXTENDING SW TO 23N60W AND ACROSS HISPANIOLA THEN INTO THE WRN CARIBBEAN. SCATTERED SHOWERS ARE WITHIN 90 NM ON EITHER SIDE OF THE FRONT. IN THE WAKE OF THE FRONT...A 1027 MB SURFACE HIGH IS CENTERED NEAR 32N73W WITH BROKEN TO OVERCAST STRATOCUMULUS CLOUDS ACROSS THE BAHAMAS AND W ATLC. RELATIVELY TRANQUIL WEATHER IS NOTED OVER THE REMAINDER OF THE ATLANTIC WITH A LARGE 1026 MB HIGH CENTERED NEAR 28N36W. ACROSS THE FAR NERN ATLC...A WEAKENING COLD FRONT CLIPS 32N11W 30N18W TO 31N26W. ISOLATED SHOWERS ARE EMBEDDED WITHIN MULTI-LAYERED CLOUDS ACROSS THE CANARY AND MADEIRA ISLANDS. ALOFT...AN UPPER LEVEL RIDGE IS CENTERED NEAR 25N43W IN THE CENTRAL ATLC WITH AN ELONGATED AND NARROW UPPER LEVEL TROUGH TO THE SE WITH AXIS ALONG THE WRN COAST OF AFRICA TO AN UPPER-LEVEL LOW NEAR 18N30W TO 12N43W. $$ HUFFMAN